Soil Types Classification and Testing

Understanding what type of soil is present is important because it determines what type of plant will be most suited to an area.

This can accurately predict yields of crops for agriculture.

This can also allow for different crops to be planted that will make the most money for farmers.

Soil Classification

There are two major systems: 1) Vernacular system 2) Scientific system

Systems to Soil Classification

Vernacular system was developed by land users.

For example, in vernacular system soil can be categorized as red soil, black soil, yellow soil, etc.

These classifications determine what the soil can be used for.

Very general, not scientific. Mostly based on colour and what is growing

well in the soil at the time it is tested.

Vernacular System

In the scientific system, the soil can be categorized according to:◦ the development of soil

(how was it created?) ◦ the amount of

substances present in the soil (what is the ratio of organic matter, water, air and minerals?)

Scientific System

As there are various systems to classify soils, it means soil classification is not static or has 1 way of going about it.

However, most classification of soil is based on the size of the particles it contains.

This classification helps to understand the basic properties of the soil and helps to conclude if the type of soil is good enough for gardening or farming

Particle Classification

Therefore depending on the size of the particles in the soil, it can be classified into these following main types: ◦ Sandy soil◦ Silty soil◦ Clay soil

Types of Soil

This soil type has the biggest particles. This creates better aeration and drainage of the

soil. This soil is granular and consists of rock and

mineral particles that are very small, creating a gritty texture.

Sandy soil is formed when rocks such as limestone, granite, quartz and shale are weathered.

Sandy soil is easier to grow on if it is rich in organic material, but can also allow for too much drainage.

This can create over-drainage and dehydration of the plants in summer.

Sandy Soil

To check if soil is sandy, moisten a small sample of soil and try to make a ball using your palms.

If the soil is sandy, then no dirt balls will form and the soil will crumble and fall through the fingers.

Testing for sandy soil:

Silty soil is considered to be one of the most fertile of soils.

It can occur in nature as soil, or is often found at the bottom of lakes or rivers.

It is composed of minerals like quartz and fine organic particles.

More nutrients than sandy soil and offers better drainage.

If it is fully dry it can look like dark sand.

Silty Soil

To check if the soil you have is silty, take a small amount of moist soil and rub it between your fingers.

If the soil is silty soil, it will feel slick and stick to your fingers.

Testing for Silty Soil:

Clay is a kind of material that occurs naturally and consists of very fine grain material with less air spaces.

It is difficult to work with this soil, because the drainage in this soil is low.

Soil can become water logged and damage roots. Very heavy when wet and lots of fertilizers need to

be added. Clay soil is formed after years of rock weathering. Rich in mineral content.

Clay Soil

To identify if the soil is clay soil, take a soil sample and damp it with water.

Rub it between your palms. You will find clay soil is sticky and retains a

good amount of water.

Testing for Clay soil

Sandy, silty and clay soil are the 3 main types.

There are subtypes, which are not as easy to test for.

These subtypes are:◦ Loamy soil◦ Peaty soil◦ Chalky soil

Types of Soil

This soil consists of sand, silt and clay to some extent.

It is considered to be the perfect soil for gardening.

The texture is gritty and retains water very easily, yet the drainage is good.

There are various kinds of loamy soil ranging from fertile to very muddy and thick sod.

Ideal for cultivation. Good for vegetable patches or gardens

Loamy Soil

This kind of soil is basically formed by the accumulation of dead and decayed organic matter, it naturally contains much more organic matter than most of the soils.

It is generally found in marshy areas. Decomposition is very slow because peat is naturally

acidic. This can preserve materials. This kind of soil is formed in wet climate. Though the soil is rich in organic matter, nutrients

present are fewer in this soil type than any other type because of the slow decomposition.

Usually added to basic soil to increase water retention.

Peaty Soil

Basic (alkaline) in nature, opposite to peaty soil. Can have a large number of stones. A lot of watering and fertilizer needed to grow plants well. Also blocks the nutritional elements for the plants like iron

and magnesium.

Chalky Soil

In this classification, soil is either acidic or alkaline soil depending on the amount of humus (completely broken down organic matter), organic matter and the underlying bedrock/parent material.

pH of soils

All materials have a pH level. This determines how acidic or basic

(alkaline) a material is. If something is acidic, it will have more

hydrogen (H) in it. If something is basic, it will have more

hydroxide (OH) in it.

pH Scale

Most plants prefer a pH level of 5.8-6.2. In Manitoba, our water is closer to 7. Therefore, sometimes acids have to be

added to soil to decrease the pH to a more acidic level.

This can be done through fertilizers and solutions.

This also depends on the specific plant and the pH of the soil itself.